Articles | Volume 21, issue 10
https://doi.org/10.5194/hess-21-5165-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-21-5165-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Convective rainfall in a dry climate: relations with synoptic systems and flash-flood generation in the Dead Sea region
Idit Belachsen
CORRESPONDING AUTHOR
Hydrology and Water Resources Program, Hebrew University of Jerusalem, 91904, Israel
Institute of Earth Sciences, Hebrew University of Jerusalem, 91904, Israel
Francesco Marra
Institute of Earth Sciences, Hebrew University of Jerusalem, 91904, Israel
Nadav Peleg
Institute of Environmental Engineering, Hydrology and Water Resources Management, ETH Zurich, Switzerland
Institute of Earth Sciences, Hebrew University of Jerusalem, 91904, Israel
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- An idealized model sensitivity study on Dead Sea desertification with a focus on the impact on convection S. Khodayar & J. Hoerner 10.5194/acp-20-12011-2020
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- Impacts of Non-Local versus Local Moisture Sources on a Heavy (and Deadly) Rain Event in Israel B. Lynn et al. 10.3390/atmos12070855
- Linking frequency of rainstorms, runoff generation and sediment transport across hyperarid talus‐pediment slopes Y. Shmilovitz et al. 10.1002/esp.4836
- Hydroclimatic variability of opposing Late Pleistocene climates in the Levant revealed by deep Dead Sea sediments Y. Ben Dor et al. 10.5194/cp-17-2653-2021
- Direct, continuous measurements of ultra-high sediment fluxes in a sandy gravel-bed ephemeral river K. Stark et al. 10.1016/j.geomorph.2021.107682
- Reduced Rainfall in Future Heavy Precipitation Events Related to Contracted Rain Area Despite Increased Rain Rate M. Armon et al. 10.1029/2021EF002397
- Mapping seasonal and annual extreme precipitation over the Peruvian Andes F. Domínguez-Castro et al. 10.1002/joc.5739
- Radar-based characterisation of heavy precipitation in the eastern Mediterranean and its representation in a convection-permitting model M. Armon et al. 10.5194/hess-24-1227-2020
- Hydrological modelling in desert areas of the eastern Mediterranean D. Zoccatelli et al. 10.1016/j.jhydrol.2020.124879
- Modeling of rainfall–runoff events using HEC-HMS model in southern catchments of Jerusalem Desert-Palestine M. Shakarneh et al. 10.1007/s12517-021-09406-z
- Synoptic-Scale Control over Modern Rainfall and Flood Patterns in the Levant Drylands with Implications for Past Climates M. Armon et al. 10.1175/JHM-D-18-0013.1
- Modelling of the Discharge Response to Climate Change under RCP8.5 Scenario in the Alata River Basin (Mersin, SE Turkey) Ü. Yıldırım et al. 10.3390/w13040483
- Bayesian Regularized Neural Network Model Development for Predicting Daily Rainfall from Sea Level Pressure Data: Investigation on Solving Complex Hydrology Problem L. Ye et al. 10.1155/2021/6631564
- Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins D. Zoccatelli et al. 10.5194/hess-23-2665-2019
- Evident response of future hydropower generation to climate change J. Li et al. 10.1016/j.jhydrol.2020.125385
- Temperature effects on the spatial structure of heavy rainfall modify catchment hydro-morphological response N. Peleg et al. 10.5194/esurf-8-17-2020
- Overview of modern atmospheric patterns controlling rainfall and floods into the Dead Sea: Implications for the lake's sedimentology and paleohydrology M. Armon et al. 10.1016/j.quascirev.2019.06.005
- Frequency analysis of storm-scale soil erosion and characterization of extreme erosive events by linking the DWEPP model and a stochastic rainfall generator Y. Shmilovitz et al. 10.1016/j.scitotenv.2021.147609
- Controls of flash flood peak discharge in Mediterranean basins and the special role of runoff-contributing areas Y. Rinat et al. 10.1016/j.jhydrol.2018.08.055
- A simplified MEV formulation to model extremes emerging from multiple nonstationary underlying processes F. Marra et al. 10.1016/j.advwatres.2019.04.002
- Rainfall intensity in short events: Evaluating the “I30 is equal to twice the rainfall depth” approach advised for use with the Universal Soil Loss Equation by Wischmeier & Smith (1978) D. Dunkerley 10.1016/j.catena.2021.105659
- Rainfall intensity in geomorphology: Challenges and opportunities D. Dunkerley 10.1177/0309133320967893
- Runoff volume and sediment yield from an endorheic watershed generated by rare rainfall events in the Atacama Desert H. Alcayaga et al. 10.1016/j.geomorph.2021.108107
- Flash Flooding in Arid/Semiarid Regions: Climatological Analyses of Flood-Producing Storms in Central Arizona during the North American Monsoon L. Yang et al. 10.1175/JHM-D-19-0016.1
- How Is the Intensity of Rainfall Events Best Characterised? A Brief Critical Review and Proposed New Rainfall Intensity Index for Application in the Study of Landsurface Processes D. Dunkerley 10.3390/w12040929
- Autocorrelation structure of convective rainfall in semiarid-arid climate derived from high-resolution X-Band radar estimates F. Marra & E. Morin 10.1016/j.atmosres.2017.09.020
- Hydrometeorological analysis and forecasting of a 3 d flash-flood-triggering desert rainstorm Y. Rinat et al. 10.5194/nhess-21-917-2021
Latest update: 23 Mar 2023
Short summary
Spatiotemporal rainfall patterns in arid environments are not well-known. We derived properties of convective rain cells over the arid Dead Sea region from a long-term radar archive. We found differences in cell properties between synoptic systems and between flash-flood and non-flash-flood events. Large flash floods are associated with slow rain cells, directed downstream with the main catchment axis. Results from this work can be used for hydrological models and stochastic storm simulations.
Spatiotemporal rainfall patterns in arid environments are not well-known. We derived properties...